{"id":41718,"date":"2021-08-07T18:59:00","date_gmt":"2021-08-07T18:59:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=41718"},"modified":"2021-08-10T21:21:48","modified_gmt":"2021-08-10T21:21:48","slug":"transverse-banding-associated-with-a-decaying-mesoscale-convective-system","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/41718","title":{"rendered":"Transverse banding associated with a decaying Mesoscale Convective System"},"content":{"rendered":"<p><\/p>\n<div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/08\/210807_goes16_waterVapor_infrared_Upper_Midwest_transverse_banding_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/08\/tb_ir-20210807_140117.png\" alt=\"GOES-16 Mid-level Water Vapor (6.9 \u00b5m) and \u201cClean\u201d Infrared Window (10.35 \u00b5m) images, with pilot reports of turbulence plotted in cyan\/yellow [click to play animation | MP4]\" width=\"640\" height=\"381\"><\/a><p class=\"wp-caption-text\">GOES-16 Mid-level Water Vapor <em>(6.9<\/em> <em>\u00b5m)<\/em>&nbsp;and \u201cClean\u201d Infrared Window <em>(10.35<\/em> <em>\u00b5m)<\/em>&nbsp;images, with pilot reports of turbulence plotted in cyan\/yellow [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/08\/210807_goes16_waterVapor_infrared_Upper_Midwest_transverse_banding_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n<p>GOES-16 <em>(GOES-East)<\/em> Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) and \u201cClean\u201d Infrared Window (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band13.pdf\"><strong>10.35 \u00b5m<\/strong><\/a>) images <strong><em>(above)<\/em><\/strong> revealed the formation of transverse banding along the eastern periphery of a decaying Mesoscale Convective System in the Upper Midwest during the morning hours on <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20210807.html\"><strong>07 August 2021<\/strong><\/a>. Transverse banding is a satellite signature that usually indicates an enhanced potential of turbulence (<a href=\"https:\/\/journals.ametsoc.org\/view\/journals\/wefo\/24\/5\/2009waf2222285_1.xml\"><strong>reference)<\/strong><\/a>&#8212; and there were indeed multiple reports of light-to-moderate turbulence within the 26-50,000 feet altitude range <em>(cyan)<\/em>.<\/p>\n\n\n<hr class=\"wp-block-separator\" \/>\n\n\n\n<p>CIMSS Scientists have used machine-learning to create a predictive tool for moderate-or-greater (MOG) turbulence based in part on satellite imagery.  The product for 1405 UTC on 7 August is shown below.  A maximum is anchored on the MCS.  This product is available online <a href=\"https:\/\/cimss.ssec.wisc.edu\/turbulence\/\">here<\/a>.  Training for this product is <a href=\"https:\/\/cimss.ssec.wisc.edu\/training\/YouTube_TurbulenceTraining.html\">here<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/probability_Midwest_20210807_1405UTC_29-41kft.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"659\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/probability_Midwest_20210807_1405UTC_29-41kft-1024x659.png\" alt=\"\" class=\"wp-image-41871\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/probability_Midwest_20210807_1405UTC_29-41kft-1024x659.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/probability_Midwest_20210807_1405UTC_29-41kft-300x193.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/probability_Midwest_20210807_1405UTC_29-41kft-768x495.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2021\/08\/probability_Midwest_20210807_1405UTC_29-41kft.png 1250w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption>Probability of Moderate-or-Greater turbulence, 1405 UTC on 7 August 2021 (Click to enlarge)<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) Mid-level Water Vapor (6.9 \u00b5m) and \u201cClean\u201d Infrared Window (10.35 \u00b5m) images (above) revealed the formation of transverse banding along the eastern periphery of a decaying Mesoscale Convective System in the Upper Midwest during the morning hours on 07 August 2021. Transverse banding is a satellite signature that usually indicates an enhanced potential [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":41814,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[21,74],"tags":[],"class_list":["post-41718","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aviation","category-goes-16"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/41718","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/users\/18"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=41718"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/41718\/revisions"}],"predecessor-version":[{"id":41873,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/41718\/revisions\/41873"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/41814"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=41718"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=41718"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=41718"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}